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Updated: Mar 18, 2026

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
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Published on: August 5, 2016

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中洋山頂の地震性は,極端なタイプの海洋石層を明らかにします

Vera Schlindwein1, Florian Schmid1

  • 1Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Am Alten Hafen 26, 27568 Bremerhaven, Germany.

Nature
|July 1, 2016
PubMed
まとめ

地震データによると,超低速に広がる山脊には冷たい,厚い石層があり,深い地震は広範囲の蛇形化を示しています. これは地殻の不連続な生成と 深い液体の循環を説明します

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